Articles | Volume 21, issue 11
https://doi.org/10.5194/acp-21-8655-2021
© Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License.
The impact of aerosol size-dependent hygroscopicity and mixing state on the cloud condensation nuclei potential over the north-east Atlantic
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- Final revised paper (published on 08 Jun 2021)
- Supplement to the final revised paper
- Preprint (discussion started on 09 Feb 2021)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on acp-2021-96', Anonymous Referee #1, 10 Mar 2021
- AC2: 'Reply on RC1', Wei Xu, 05 May 2021
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RC2: 'Comment on acp-2021-96', Anonymous Referee #2, 18 Apr 2021
- AC1: 'Reply on RC2', Wei Xu, 05 May 2021
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Wei Xu on behalf of the Authors (05 May 2021)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (13 May 2021) by Alexander Laskin
AR by Wei Xu on behalf of the Authors (13 May 2021)
Manuscript
This study presents data collected from the Mace Head field operational site and presents an analysis of the influence of the size-dependent hygroscopicity and mixing state of aerosols for the prediction of the CCN number. The authors compare CCN number closure using 6 different methods on aerosol concentrations measured over Northeast Atlantic. The work provides significant long-range measurement of CCN from one site. The sampled air masses are divided into sectors, including polluted continent, clean oceanic, and mixtures for both high and low biological level of activity. It was concluded that for low SS the mixing state plays an important role while for high SS the hygroscopicity is size dependent.
The paper is appropriate for submission to ACP. The issue of NCCN closure is of scientific importance and thus the work contributes new data and methods of scientific significance to the field. There are several grammatical errors and typo through the manuscript. There are some questions regarding the approach and interpretation of the analytical methods D-F. There are also additional questions regarding the relevance/reliance on data provided in the supplemental document for the understanding of the main manuscript.
Overall, the manuscript and contents continue the important scientific discussion about NCCNprediction and should be published. This reviewer congratulates the authors on synthesizing a significantly large and complex CCN measurement and prediction data set. There are several unique features that can be discerned over a long period of time and the authors have overall presented a cohesive narrative that expands our knowledge of CCN prediction and the aerosol-indirect effect.
Below are some major and minor comments that are suggested to improve the clarity of the work.
Major Comments:
Minor Comments:
Line 15-16: Please check method description. “Method C utilized size dependent…” Isn’t this D?
Line 27: GF-PDf or GF-PDF?
Line 33: supersaturation vs super-saturation (line 11)
Line 51: nss-sulfate is not defined until line '154.
Line 147: arbitrary? Mixing State can be quantified. Please see Riemer, N., et al
Line 159: the letter d is missing from "and", “ammonium nitrate an sulfate”
Line 188: Please be aware that the font size and notation in the subscripts is not consistent. Similar inconsistencies can be found on other pages as well (pg 7, 8, so on and so forth).
Table 1: It is not clear in the criteria in the table if it is and/or. For example, BC< 15 ng AND WD from? Or is it one or the other?
Line 205: Please reword “were taking into”. Take into?
Page 8: The alignment of the columns in Table 2 is awkward. Perhaps centering?
Table 2: Is a reference for the density of organics required? What is the justification for 1400.
Line 239-240 why is the upper limit 500nm? Is 500nm the limitation in the DMA measurement?
Line 269: Change “In method F” to “In method E”.
Line 339 lend support “to”?
Line 343: Typo. Change to “Respectively”.
Line 343: HB and LB not defined.
Llne 355: "Fig 4&-5"?
Line 356: This range is peculiar. The minimum value of Pearson’ coefficient does not seem to be 0.85 (more like 0.76 in fig. 4 and 0.65 in fig. 5).
Line 361: Sentence is unclear.
Line 373, 380-381: Please double check ranges. The slope and R minimum and maximum values mentioned here do not match the ones written on the panels in fig. 4.
Line 423: The word “eith” is likely misspelt.
Line 454 “That indicated the potential over-estimation of 30% to 50% by using κ of 0.3 in highly polluted air masses” Is kappa or Nccn overestimated 30~50%?
Line 473: Change "compare" to compared
Line 485 “To conclude, using κ of 0.3 achieved reasonable closure in Polluted-H but resulted in significant over-estimation in Polluted-L by up to 50 to 60% and using bulk PM1 chemical composition enabled to achieve closure in Polluted-H, but showed over-estimation in Polluted-L.” What is enabled to achieve? Simply achieved?
Line 539: verb tense? Commonly adapted practice(s).
line 541: Please rephrase ‘pointing size mattered most at CCN activation.’ Indicating that?
Line 589: Reduced the error by 80% with respect to what?
REFERENCES:
Riemer, N., et al. "Aerosol mixing state: measurements, modeling, and impacts." Reviews of Geophysics 57.2 (2019): 187-249.